Fig. 8From: The sensitivity of ocean tide loading displacements to the structure of the upper mantle and crust of Taiwan IslandUnit thickness sensitivity kernels of the modeled M2 OTL displacements. The modeled M2 OTL displacements are predicted at 24.5°N on Taiwan Island to + 10% linear perturbations of the density (left), bulk modulus (middle), and shear modulus (right) in the upper crust (black), middle crust (green), lower crust (blue), LID (magenta), LVZ (red), and region above the transition zone (yellow) of TW1. The depths of the perturbed layers: the upper crust (0–13.88 km depth), middle crust (13.88–24.52 km depth), lower crust (24.52–32.15 km depth), LID (32.15–80 km depth), LVZ (80–220 km depth), and region above the transition zone (220–400 km depth)Back to article page